High‐pressure micro‐inclusions and development of an inverted metamorphic gradient in the Santiago Schists (Ordenes Complex, NW Iberian Massif, Spain): evidence of subduction and syncollisional decompression

  1. ARENAS, R.
  2. PASCUAL, F.J.R.
  3. GARCIA, F.D.
  4. CATALAN, J.R.M.
Revista:
Journal of Metamorphic Geology

ISSN: 1525-1314,  0263-4929

Ano de publicación: 1995

Volume: 13

Número: 2

Páxinas: 141-164

Tipo: Artigo

DOI: 10.1111/J.1525-1314.1995.TB00211.X GOOGLE SCHOLAR
Fonte de datos: Scopus